Clay is made of very small bits of mineral, which are made when rocks erode. The mineral particles in clay are much smaller than sand or silt, which is why clay can hold so much water: the water molecules stick in between tiny thin layers of clay molecules.
Loam is a soil that’s a mix of lots of different materials, including sand, silt, clay, and organic matter.
It’s the size of the particles. Clay particles are so fine that you can’t feel them with your fingers so it feels smooth. Only certain minerals are even capable of being so fine. These “clay minerals” also tend to have a very thin plate-like shape under a microscope. Because the particles have a flat shape, they have a lot of surface area, so they have a tendency to be really cohesive and stick together.
As a young man I worked as a soils mechanic for a construction company.
Clay is flat particles smaller than 200 parts per inch. Silt is round particles, smaller than 200 parts per inch.
Dirt is what gets swept up when you clean the floor. Soil is all of the stuff that you see when you dig into the ground.
Clay is sticky because when they get wet, the flat particles stick to one another. Round particles do not stick together.
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